(Fig. 4) Relative proportions of the most abundant chironomid taxa in the Lake Temje sediment core
| Cobertura |
LATITUDE: 62.050000 * LONGITUDE: 129.483300 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 3.70 m |
|---|---|
| Data(s) |
25/11/2013
|
| Formato |
text/tab-separated-values, 168 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.802678 doi:10.1594/PANGAEA.802678 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.802679 Nazarova, Larisa B; Lüpfert, Herman; Subetto, Dmitry A; Pestryakova, Ludmila A; Diekmann, Bernhard (2013): Holocene climate conditions in central Yakutia (Eastern Siberia) inferred from sediment composition and fossil chironomids of Lake Temje. Quaternary International, 290-291, 264-274, doi:10.1016/j.quaint.2012.11.006 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AWI_PerDyn; Calculated after Shannon (1948); Central Yakutia, Russia; Chironomidae, larvae, head capsules of dry mass; DEPTH, sediment/rock; Diversity; Evenness of species; Lake_Temje; Number of species; Periglacial Dynamics @ AWI; RPC; Russian peat corer |
| Tipo |
Dataset |
